This paper discusses the history of atmospheric lead pollution, the past ge
ographic distribution of atmospheric lead deposition in Sweden, and the fat
e of the pollution lead in boreal forest soils. The paper is based on analy
ses of Pb-206/Pb-207 isotope ratios and lead concentrations in lake sedimen
ts, peat deposits and soil profiles from Sweden. The first signs of atmosph
eric lead pollution date back to 3500 to 4000 years ago. There was a small,
but clear peak during the Greek-Roman period around 0 AD. About 1000 AD a
major and unreversed increase occurred; varved lake sediments disclose poll
ution peaks at about 1200 AD and 1530 AD, which match peaks in metallurgy i
n Europe. With the Industrial Revolution atmospheric lead pollution increas
ed, however, not as much as usually suggested, and not at all from what can
be called background values. Lead pollution increased markedly after World
War II, peaked about 1970, and will, if the present trend continues, soon
be back to Medieval levels. The distribution of pre-industrial pollution wa
s similar to the contemporary pattern with a strong south to north gradient
, as a result of northward atmospheric transport from continental Europe an
d the British Isles. The cumulative load of pollution lead through time is
2 to 3 g m(-2) in S Sweden, and of this load at least 50% was deposited pri
or to 1800 AD. In boreal forest soils, the main part of this pollution lead
has accumulated in the B horizon. Present-day concentrations in the mor la
yer are up to 1000 times higher than in the pristine forest prior to pollut
ion.